{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361418519126582016.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/ee-1-23-2006"}},{"identifier":{"@type":"URI","@value":"http://www.electronic-earth.net/1/23/2006/ee-1-23-2006.pdf"}},{"identifier":{"@type":"DOI","@value":"10.5194/eed-1-135-2006"}},{"identifier":{"@type":"URI","@value":"http://www.electronic-earth-discuss.net/1/135/2006/eed-1-135-2006.pdf"}}],"dc:title":[{"@value":"Earthquake fault rock indicating a coupled lubrication mechanism"}],"description":[{"notation":[{"@value":"A pseudotachylyte bounded by a carbonate-matrix implosion breccia was found at a fossilized out-of-sequence thrust in the Shimanto accretionary complex, Japan. This occurrence resulted from the following events: first implosion of host rock due to interstitial fluid pressure increase and asymmetric fracturing; second, Ca-Fe-Mg carbonate precipitation; and third, frictional melting. The rock-record suggests that these events took place in a single seismogenic slip event. Resulting from abrupt drop in fluid pressure after implosion, hydro-fracturing and fluid escape, recovered high effective friction promoted melting during fault movement. Coexistence of fluid implosion breccia and pseudotachylyte has never been reported from continental pseudotachylytes, but might be characteristic from hydrous seismogenic faults in subduction zones."}]},{"notation":[{"@value":"International audience"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285532845465349","@type":"Researcher","foaf:name":[{"@value":"S. Okamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418519126582016","@type":"Researcher","foaf:name":[{"@value":"G. Kimura"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418519126582017","@type":"Researcher","foaf:name":[{"@value":"S. Takizawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418519126582019","@type":"Researcher","foaf:name":[{"@value":"H. Yamaguchi"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1893961342981893764","@type":"Researcher","foaf:name":[{"@value":"The Institute for Frontier Research on Earth Evolution ; Japan Agency for Marine-Earth Science and Technology (JAMSTEC)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893961342981893766","@type":"Researcher","foaf:name":[{"@value":"Institute of Geoscience ; Université de Tsukuba = University of Tsukuba"}]},{"@id":"https://cir.nii.ac.jp/crid/1893961342981893763","@type":"Researcher","foaf:name":[{"@value":"Department of Earth and Planetary Science [Tokyo] ; Graduate School of Science [Tokyo] ; The University of Tokyo (UTokyo)-The University of Tokyo (UTokyo)"}]},{"@id":"https://cir.nii.ac.jp/crid/1891710641388032260","@type":"Researcher","foaf:name":[{"@value":"EGU, Publication"}]},{"@id":"https://cir.nii.ac.jp/crid/1891710641388032258","@type":"Researcher","foaf:name":[{"@value":"Graduate School of Science Tokyo"}]},{"@id":"https://cir.nii.ac.jp/crid/1891710641388032263","@type":"Researcher","foaf:name":[{"@value":"Department of Earth and Planetary Science Tokyo"}]},{"@id":"https://cir.nii.ac.jp/crid/1891710641388032257","@type":"Researcher","foaf:name":[{"@value":"The Institute for Frontier Research on Earth Evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1891710641388032262","@type":"Researcher","foaf:name":[{"@value":"The University of Tokyo (UTokyo)-The University of Tokyo (UTokyo)"}]},{"@id":"https://cir.nii.ac.jp/crid/1891710641388032261","@type":"Researcher","foaf:name":[{"@value":"Japan Agency for Marine-Earth Science and Technology (JAMSTEC)"}]},{"@id":"https://cir.nii.ac.jp/crid/1891710641388032259","@type":"Researcher","foaf:name":[{"@value":"Institute of Geoscience"}]},{"@id":"https://cir.nii.ac.jp/crid/1891710641388032256","@type":"Researcher","foaf:name":[{"@value":"Université de Tsukuba = University of Tsukuba"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18153828"},{"@type":"EISSN","@value":"18153844"}],"prism:publicationName":[{"@value":"eEarth"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2006-12-20","prism:volume":"1","prism:number":"1","prism:startingPage":"23","prism:endingPage":"28"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://www.electronic-earth.net/1/23/2006/ee-1-23-2006.pdf"},{"@id":"http://www.electronic-earth-discuss.net/1/135/2006/eed-1-135-2006.pdf"}],"createdAt":"2010-04-29","modifiedAt":"2011-06-10","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences","dc:title":"[SDU.STU] Sciences of the Universe [physics]/Earth Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences","dc:title":"[SDU.STU]Sciences of the Universe [physics]/Earth Sciences"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002216707264896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimental investigation of frictional melting of argillite at high slip rates: Implications for seismic slip in subduction‐accretion complexes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229800450944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contrasts in physical properties between the hanging wall and footwall of an exhumed seismogenic megasplay fault in a subduction zone—An example from the Nobeoka Thrust Drilling 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